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Kallimorphocrinus eaglei
Taxonomy
Isoallagecrinus eaglei was named by Strimple (1966). Its type specimen is OU 4993 and is a 3D body fossil. Its type locality is Southeastern part of Burbank Stone Company quarry, which is in an Asselian open shallow subtidal limestone in the Red Eagle Limestone Formation of Oklahoma.
It was recombined as Kallimorphocrinus eaglei by Webster and Lane (2007).
It was recombined as Kallimorphocrinus eaglei by Webster and Lane (2007).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1966 | Isoallagecrinus eaglei Strimple p. 105 figs. Pl 1, figs 1-3 |
| 1967 | Isoallagecrinus eaglei Webster and Lane p. 11 figs. Pl 3, figs 9,10 |
| 2007 | Kallimorphocrinus eaglei Webster and Lane p. 954 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Kallimorphocrinus eaglei Strimple 1966
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: subc = subclass, c = class, p = phylum | |||||
| References: Aberhan et al. 2004, Aberhan 1992, Kiessling 2004 | |||||
Age range: base of the Asselian to the top of the Artinskian or 298.90000 to 283.30000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Asselian | USA (Oklahoma) | Isoallagecrinus eaglei (151347) | |
| Artinskian | USA (Nevada) | Isoallagecrinus eaglei (90756) |